Vector empirical orthogonal function modes of the ocean surface wind variability derived from satellite scatterometer data

Ocean surface winds derived from NSCAT, QuikSCAT and ERS-1/2 scatterometer observations during a period from January 1992 to April 2000 were analyzed using the vector empirical orthogonal function (VEOF) method. With the bore al winter and summer oscillation, the first VEOF is dominated by the Indian and East Asian monsoons and also shows an annual cycle of the trade winds. The second VEOF represents the boreal autumn and spring oscillation, and r eveals a transition state between winter and summer. The third VEOF indicat es the wind variability associated with El Nino Southern Oscillation (ENSO) events, because the temporal mode has a high correlation coefficient of 0. 8 with the Southern Oscillation Index (SOI). Further more, the third mode r eveals the teleconnection of the Indian monsoon and wind variability over h igh latitude oceans', such as the Aleutian Low system, with ENSO events.